Sheepeater Canyon spring (Yellowstone)
Yellowstone National Park, Wyoming, United States
Other media
- Type
- Other medium
Hydrothermal system of the Yellowstone caldera. Palmer and Sturchio (1990): waters from -9.3 to +4.4 ‰; Norris and Upper Geyser basins, Calcite Springs and Clearwater stay close to fresh rhyolite (-5.2 ‰), Mammoth, Sheepeater and Rainbow near -8 ‰, like altered rhyolite (-9.7 ‰) or sediments outside the caldera.
δ11B in ‰ (per mil) Values of the same system
Standard : NIST SRM 951
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| −9.3 ‰ | 1 | thermal water Single analysis (Y88-8 Sheepeater Canyon). Y88-8 Sheepeater Canyon: 73 °C, pH (7.0), B 0.21 mmol/kg, Cl 2.6 mmol/kg (pH in brackets measured in the laboratory). | Palmer & Sturchio (1990), The boron isotope systematics of the Yellowstone National Park … |
Deposits of the same type
Cite this page
IsoFind Atlas (2026). Sheepeater Canyon spring (Yellowstone), isotope signatures. https://www.isofind.tech/isotopes/en/sites/source-de-sheepeater-canyon-yellowstone/ (accessed 2026-10-20).
@misc{isofind2026sheepeatercanyonspringyellows,
title = {Sheepeater Canyon spring (Yellowstone), isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/sites/source-de-sheepeater-canyon-yellowstone/},
note = {Accessed 2026-10-20}
}Updated : 2026-10-20